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Learn more about these natural ice formations
Definition of a glacier: A glacier is a slow-moving mass of ice that forms over centuries when snow accumulates and compresses. They shape landscapes and impact climate.
Glaciers are Earth’s slow-moving rivers of ice, carving valleys, shaping mountains, and storing freshwater. But what exactly are they and how do they form?
Glaciers are among the most fascinating natural wonders of our planet. Glaciers are found in areas where the annual snowfall exceeds the rate at which the snow melts. This process can take hundreds to thousands of years, resulting in vast, thick ice formations.
Alpine Glaciers: Also known as mountain glaciers, these are found in high mountainous regions. They flow down valleys and can form spectacular landscapes, such as U-shaped valleys and fjords. Glaciers in Norway are Alpine Glaciers.
Continental Glaciers: These are larger and cover extensive land areas. The two remaining ice sheets, found in Greenland and Antarctica, are prime examples. These ice sheets are so massive that they hold most of the Earth’s freshwater reserves.
Jostedalsbreen Glacier in Norway. Photo: Thomas T. Kleiven - VisitNorway.com
The formation of glaciers begins with snowflakes, which compact under the weight of new snowfall. Over time, the compacted snow turns into firn, a granular type of snow. With continued compression, firn becomes dense glacial ice.
Glaciers move due to gravity and their immense weight. This movement occurs through two main processes:
Internal Deformation: The ice within the glacier deforms and flows slowly.
Basal Sliding: The glacier slides over the bedrock, lubricated by a thin layer of meltwater at its base.
Kayaking near the Folgefonna Glacier in Norway. Photo: Fjord Norway
Glaciers have a profound impact on the Earth’s topography. Their movement carves out valleys, shapes mountains, and transports vast amounts of rock and debris. When glaciers retreat, they leave behind unique landforms such as moraines, eskers, and drumlins. The Norwegian fjords was created by glaciers that made U-shaped valleys by segregation through several ice ages. The valleys were then filled with water from the sea. You can read more about Norwegian fjords here.
It depends a bit on how you count, how you divide the glaciers, and what is included. A common number is 2,534 glaciers in Norway if you look at a report from NVE from 2022.
Looking at glaciers divided into ice sections, there are 38 glaciers with an area over 10 km². If you include all glaciers over 0.1 km², there are a total of 1,678 glaciers.
These glaciers cover about 2,600 square kilometers and are primarily located in the western and northern parts of the country.
Ice melting could cause the glacier to divide and split into different sections, potentially increasing the count of individual sections even as the total square meters of the glacier decreases.
Bergen is the second largest city in Norway, located on the west coast surrounded by the Norwegian Fjords Sognefjorden in the north and Hardangerfjorden in the south. The closest glacier to visit is Folgefonna and you can reach the glacier on a day trip from Bergen. However, we do recommend spending a few days in the region around the glacier to get the full experience. The village Rosendal one hour from the glacier is a perfect place to include in your glacier visit.
When exploring the beautiful landscapes of glaciers, understanding and prioritizing safety is essential for ensuring a successful and memorable experience. Please take note of the following safety tips:
Q: How fast do glaciers move?
A: Most glaciers move a few centimeters per day, but some surge several meters in rare events.
Q: Can you walk on a glacier in Norway?
A: Yes, but only with a certified guide, as hidden crevasses make it dangerous.
Norway’s glaciers are breathtaking but rapidly disappearing. Whether you visit Folgefonna or Jostedalsbreen, exploring these icy giants offers a glimpse into our planet’s past – and future.
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